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  2. Aeolian processes - Wikipedia

    en.wikipedia.org/wiki/Aeolian_processes

    Winds may erode, transport, and deposit materials and are effective agents in regions with sparse vegetation, a lack of soil moisture and a large supply of unconsolidated sediments. Although water is a much more powerful eroding force than wind, aeolian processes are important in arid environments such as deserts. [2]

  3. Aeolian landform - Wikipedia

    en.wikipedia.org/wiki/Aeolian_landform

    Aeolian landforms, or Eolian landforms, are produced by either the erosive or depositive action of wind. These features may be built up from sand or snow , [ 1 ] or eroded into rock, snow, or ice. Aeolian landforms are commonly observed in sandy deserts and on frozen lakes or sea ice and have been observed and studied around Earth and on other ...

  4. Sediment transport - Wikipedia

    en.wikipedia.org/wiki/Sediment_transport

    Aeolian or eolian (depending on the parsing of æ) is the term for sediment transport by wind. This process results in the formation of ripples and sand dunes. Typically, the size of the transported sediment is fine sand (<1 mm) and smaller, because air is a fluid with low density and viscosity, and can therefore not exert very much shear on ...

  5. Placer deposit - Wikipedia

    en.wikipedia.org/wiki/Placer_deposit

    The name is from the Spanish word placer, meaning "alluvial sand". Placer mining is an important source of gold, and was the main technique used in the early years of many gold rushes, including the California Gold Rush. Types of placer deposits include alluvium, eluvium, beach placers, aeolian placers and paleo-placers. [2]

  6. Eolianite - Wikipedia

    en.wikipedia.org/wiki/Eolianite

    Eolianite or aeolianite is any rock formed by the lithification of sediment deposited by aeolian processes; that is, the wind. In common use, however, the term refers specifically to the most common form of eolianite: coastal limestone consisting of carbonate sediment of shallow marine biogenic origin, formed into coastal dunes by the wind, and ...

  7. Parent material - Wikipedia

    en.wikipedia.org/wiki/Parent_material

    Parent material is the underlying geological material (generally bedrock or a superficial or drift deposit) in which soil horizons form. Soils typically inherit a great deal of structure and minerals from their parent material, and, as such, are often classified based upon their contents of consolidated or unconsolidated mineral material that has undergone some degree of physical or chemical ...

  8. Dune - Wikipedia

    en.wikipedia.org/wiki/Dune

    Cross-bedding in lithified aeolian sand dunes preserved as sandstone in Zion National Park, Utah. A lithified (consolidated) sand dune is a type of sandstone that is formed when a marine or aeolian sand dune becomes compacted and hardened. Once in this form, water passing through the rock can carry and deposit minerals, which can alter the ...

  9. Category:Aeolian deposits - Wikipedia

    en.wikipedia.org/wiki/Category:Aeolian_deposits

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